中国科学院机构知识库网格
Chinese Academy of Sciences Institutional Repositories Grid
Petrology and zircon U-Pb dating of the Neoarchean scapolite-garnet calc-silicate from the Namakkal Block of the Southern Granulite Terrain, India, and their geological implications

文献类型:期刊论文

作者Zhou Feng2; Gou LongLong2; Zhai MingGuo1,2; Zhang ChengLi2; George, Paul Mathews2; Lu LunSheng2; Zhao Yan2; Ao WenHao2
刊名ACTA PETROLOGICA SINICA
出版日期2021-04-01
卷号37期号:4页码:1213-1234
关键词Scapolite-garnet calc-silicate Phase equilibrium modeling Charnockite Metasomatism The Southern Granulite Terrain India
ISSN号1000-0569
DOI10.18654/1000-0569/2021.04.15
英文摘要Granulite terranes are considered as windows open to the lower crustal processes of the Earth. In this paper, we present detailed petrology, zircon U-Pb dating and phase equilibrium modeling of scapolite-garnet calc-silicate samples from the Tammampatti area of the Namakkal Block, Southern Granulite Terrain, India. On the basis of petrographic observation, two stages of metamorphic mineral assemblages were determined, which are garnet + scapolite + plagioclase + sphene + ilmenite (M1) and epidote corona + the symplectite of calcite, plagioclase and quartz. Cathodoluminescence (CL) imaging reveals that there are two types of metamorphic zircons: zircons with high luminescence and another is characterized by low luminescence. Zircon U-Pb dating using LA-ICP-MS yielded a weighted mean Pb-207/Pb-206 age of 2562 +/- 17Ma for the zircons with high luminescence, whereas those with low luminescence have a weighted mean Pb-207/Pb-206 age of 2495 +/- 15 Ma. The peak metamorphic conditions of two samples 18ID-24 and 18ID-25 are constrained to be 800 similar to 960 degrees C/4.3 similar to 7.1 kbar and 750 similar to 854 degrees C/4.0 similar to 7.8 kbar, respectively. The metamorphic age of 2562 +/- 17Ma is the similar as the crystallization age of the charnockite pluton within the Namakkal Block, which is interpreted to represent the timing of contact metasomatism caused by magma emplacement of the charnockite. The metamorphic age of 2495 +/- 15Ma is considered to be the overprinted time by the previously reported ca. 2530 similar to 2440Ma regional HT-UHT metamorphism. The calc-silicate should be resulted from metasomatism of intermediate-acid pluton (protolith of charnockite) and carbonatite.
WOS关键词ULTRAHIGH-TEMPERATURE METAMORPHISM ; PRINCE CHARLES MOUNTAINS ; HIGH-PRESSURE GRANULITES ; HIGH-GRADE METAMORPHISM ; WESTERN DHARWAR CRATON ; KERALA KHONDALITE BELT ; FLUID-ROCK INTERACTION ; CRUSTAL EVOLUTION ; EASTERN GHATS ; NILGIRI BLOCK
WOS研究方向Geology
语种英语
WOS记录号WOS:000653537300015
出版者SCIENCE PRESS
源URL[http://ir.iggcas.ac.cn/handle/132A11/102030]  
专题地质与地球物理研究所_岩石圈演化国家重点实验室
通讯作者Gou LongLong
作者单位1.Chinese Acad Sci, Inst Geol & Geophys, State Key Lab Lithospher Evolut, Beijing 100029, Peoples R China
2.Northwest Univ, Dept Geol, State Key Lab Continental Dynam, Xian 710069, Peoples R China
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Zhou Feng,Gou LongLong,Zhai MingGuo,et al. Petrology and zircon U-Pb dating of the Neoarchean scapolite-garnet calc-silicate from the Namakkal Block of the Southern Granulite Terrain, India, and their geological implications[J]. ACTA PETROLOGICA SINICA,2021,37(4):1213-1234.
APA Zhou Feng.,Gou LongLong.,Zhai MingGuo.,Zhang ChengLi.,George, Paul Mathews.,...&Ao WenHao.(2021).Petrology and zircon U-Pb dating of the Neoarchean scapolite-garnet calc-silicate from the Namakkal Block of the Southern Granulite Terrain, India, and their geological implications.ACTA PETROLOGICA SINICA,37(4),1213-1234.
MLA Zhou Feng,et al."Petrology and zircon U-Pb dating of the Neoarchean scapolite-garnet calc-silicate from the Namakkal Block of the Southern Granulite Terrain, India, and their geological implications".ACTA PETROLOGICA SINICA 37.4(2021):1213-1234.

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来源:地质与地球物理研究所

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